BIOLOGY 622 – FALL 2014 BASAL AMNIOTA - STRUCTURE AND PHYLOGENY WEEK – 5
BIOLOGY 622 – FALL 2014 BASAL AMNIOTA - STRUCTURE AND PHYLOGENY WEEK – I INTRODUCTION
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BIOLOGY 622 – FALL 2014 BASAL AMNIOTA - STRUCTURE AND PHYLOGENY WEEK – I INTRODUCTION ANATOMICAL DEFINITION OF AMNIOTA DIADECTOMORPHA S. S. SUMIDA
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BIOLOGY 622 – FALL 2014 BASAL AMNIOTA - STRUCTURE AND PHYLOGENY WEEK – I INTRODUCTION ANATOMICAL DEFINITION OF AMNIOTA DIADECTOMORPHA S. S. SUMIDA. BRIEF OVERVIEW OF BASAL AMNIOTA DEFINITION, PHYLOGENY, AND STRUCTURE - PowerPoint PPT Presentation
Transcript of BIOLOGY 622 – FALL 2014 BASAL AMNIOTA - STRUCTURE AND PHYLOGENY WEEK – I INTRODUCTION
BIOLOGY 622 – FALL 2014BASAL AMNIOTA - STRUCTURE AND PHYLOGENY
WEEK – IINTRODUCTION
ANATOMICAL DEFINITION OF AMNIOTADIADECTOMORPHA
S. S. SUMIDA
BRIEF OVERVIEW OF BASAL AMNIOTADEFINITION, PHYLOGENY, AND
STRUCTURE “Classic” – i.e. out of date – characterizations of Amniota often go something like this:
Class AmphibiaSuperclass Amniota
Class ReptiliaClass MammaliaClass Aves
• These groups are not phylogenetically equivalent.
• Aves is a subset of Reptilia, having evolved from theropod saurischian dinosaurs.
• Doesn’t reflect the diversity of basal reptiles.
• This class will address the two major lineages of Amniota, Reptilia and the lineage that ultimately lead to mammals, the Synapsida.
• Within Reptilia it will review the diversity of early reptiles, which encapsulates two major reptilian groups: the Eureptilia (“true reptiles”) and the lesser known but extremely diverse Parareptilia.
• We will also address the relationship of Diadectomorpha to basal Amniota, as the former is minimally a very close (extinct) relative of Amniota, or may actually be amniotes themselves.
SYNAPOMORPHIES OF AMNIOTA - I Embryological Structures*• Amnion*• Chorion*• Allantois*• (Chorioallantoic membrane)* Integumentary system• Complete loss of lateral line system *• Waterproof skin*• Horny Nails• Claws Respiratory/Disgestive Systems• Relatively enlarged lungs*• Costal (negative pressure) breathing Nervous System*• Paired Spinal Accessory (XI) Nerves*• Paired Hypoglossal (XII) Nerves* Skeletal System - AxialAtlantal pleurocentrum excluded from ventral margin of vertebral column by axial intercentrumAlternation of neural spine height in presacral vertebraeTwo pairs of sacral ribs Skeletal System - AppendicularScrew-shaped glenoidEctepicondyle of humerus well developed.Highly developed olecranon process of ulnaPisiform (neomorph)Only two manual CentraliaManual phalangeal formula: 2-3-4-5-3Calcaneus (derived from fibulare)Astragalus (fused from tibiale, intermedium and proximal central elements.Only one pedal centralPedal phalangeal formula: 2-3-4-5-4 Skeletal System - SkullLoss of intertemporal bone.Postparietals on occipital surface of skullOssified spraoccipitalPost-temporal foramen lateral to supraoccipital Skeletal System – Lower JawSingle splenial bone of lower jawSingle coronoid bone of lower jawDevelopment of retroarticular process
SYNAPOMORPHIES OF AMNIOTA - II Skeletal System - Axial• Atlantal pleurocentrum excluded from ventral margin of vertebral column by axial
intercentrum• Alternation of neural spine height in presacral vertebrae• Two pairs of sacral ribs Skeletal System - Appendicular• Screw-shaped glenoid• Ectepicondyle of humerus well developed.• Highly developed olecranon process of ulna• Pisiform (neomorph)• Only two manual Centralia• Manual phalangeal formula: 2-3-4-5-3• Calcaneus (derived from fibulare)• Astragalus (fused from tibiale, intermedium and proximal central elements.• Only one pedal central• Pedal phalangeal formula: 2-3-4-5-4 Skeletal System - SkullLoss of intertemporal bone.Postparietals on occipital surface of skullOssified spraoccipitalPost-temporal foramen lateral to supraoccipital Skeletal System – Lower JawSingle splenial bone of lower jawSingle coronoid bone of lower jawDevelopment of retroarticular process
SYNAPOMORPHIES OF AMNIOTA - II Skeletal System - Skull• Loss of intertemporal bone.• Postparietals on occipital surface of skull• Ossified spraoccipital• Post-temporal foramen lateral to supraoccipital Skeletal System – Lower Jaw• Single splenial bone of lower jaw• Single coronoid bone of lower jaw• Development of retroarticular process
SKELETAL SYNAPOMORPHIES OF AMNIOTA - II
1. Horny Nails2. Claws3. Costal (negative pressure) breathing 4. Atlantal pleurocentrum excluded from
ventral margin of vertebral column by axial intercentrum
5. Alternation of neural spine height in presacral vertebrae
6. Two pairs of sacral ribs7. Screw-shaped glenoid8. Ectepicondyle of humerus well
developed.9. Highly developed olecranon process of
ulna10. Pisiform (neomorph)11. Only two manual Centralia12. Manual phalangeal formula: 2-3-4-5-3
13. Calcaneus (derived from fibulare)14. Astragalus (fused from tibiale,
intermedium and proximal central elements).
15. Only one pedal central16. Pedal phalangeal formula: 2-3-4-5-417. Loss of intertemporal bone.18. Postparietals on occipital surface of
skull19. Ossified supraoccipital20. Post-temporal foramen lateral to
supraoccipital21. Single splenial bone of lower jaw22. Single coronoid bone of lower jaw23. Development of retroarticular process
CROWN GROUP DEFINITION OF AMNIOTA: Cannot include Diadectomorpha.
NODE-BASED DEFINITION OF AMNIOTA: Could include Diadectomropha.
FEATURES SHARED BETWEEN DIADECTOMORPHA AND AMNIOTA
1. Horny Nails2. Claws3. Costal (negative pressure) breathing 4. Atlantal pleurocentrum excluded from
ventral margin of vertebral column by axial intercentrum
5. Alternation of neural spine height in presacral vertebrae
6. Two pairs of sacral ribs7. Screw-shaped glenoid8. Ectepicondyle of humerus well
developed.9. Highly developed olecranon process of
ulna10. Pisiform (neomorph)11. Only two manual Centralia12. Manual phalangeal formula: 2-3-4-5-3
13. Calcaneus (derived from fibulare)14. Astragalus (fused from tibiale,
intermedium and proximal central elements).
15. Only one pedal central16. Pedal phalangeal formula: 2-3-4-5-417. Loss of intertemporal bone.18. Postparietals on occipital surface of
skull19. Ossified supraoccipital20. Post-temporal foramen lateral to
supraoccipital21. Single splenial bone of lower jaw22. Single coronoid bone of lower jaw23. Development of retroarticular process
INTRODUCTION TO DIADECTOMORPHA Diadectomorpha includes three families: Diadectomorpha
Family LimnoscelidaeFamily TseajaiidaeFamily Diadectidae
Limnoscelidae - monogeneric Family. There are two recognized species of Limnoscelidae: Limnoscelis paludis, and L. dynatis. Tseajaiidae - monogeneric Family. It is also monospecific, consisting of a single taxon: Tseajaia campi. Diadectidae - has had numerous taxa assigned to it over the past century.
SYNAPOMORPHIES OF DIADECTOMORPHA Diadectomorphs possess all of those defining amniote features discussed above, but also have a number of features unique to the group. These include: • Loss of intertemporal bone with intertemporal becoming
incorporated into parietal as a lateral wing of the parietal bone.
• Supraoccipital extending beyond margin of the otic capsule.
• Anteriorly directed processes of atlantal intercentrum and axial intercentrum fit into ventral grooves on basioccipital and atlantal intercentrum respectively.
• Extremely robust adductor crest of ventral surface of the femur.
Loss of intertemporal bone with intertemporal becoming incorporated into parietal as a lateral wing of the parietal bone: Note the presence of an intertemporal bone in the amphibian Seymouria, below left. However, note how it is incorporated into the parietal as a lateral flange in the diadectomorphs Tseajaia and Limnoscelis middle and below right respectively
Supraoccipital ossified and extending beyond margin of the otic capsule: For example below: Seymouria is an amphibian with no ossified supraoccipital. Notice how in the diadectomorph limnosclid Limnoscelis the wide extent of the suporaoccipital (SO).
Anteriorly directed processes of atlantal intercentrum and axial intercentrum fit into ventral grooves on basioccipital and atlantal intercentrum respectively: Atlantal intercentrum is an independent structure.
Right and left atlantal neural arches are independent structures, and do not fuse in the dorsal midline.
The axial intercentrum comes to underlie the atlantal pleurocentrum – excluding the axial pleurocenrum from ventral exposure on the underside of the vertebral column.
Anteriorly directed processes of atlantal intercentrum and axial intercentrum fit into ventral grooves on basioccipital and atlantal intercentrum respectively: A small right and left proatlas provide articulation for the atlantal neural arches with the occipital region of the skull
The axis is very robust, as is the very large neural spine.
Extremely robust adductor crest of ventral surface of the femur: Note how robust in Limnoscelis and Diadectes below:
DIVERSITY, BIOGEOGRAPHIC, AND TEMPORAL DISTRIBUTION
OF DIADECTOMORPHA
DIADECTOMORPHA
Family LimnoscelidaeGenus Limnoscelis
L. paludis Late Pennsylvanian; north-central New Mexico (southeastern Utah?)
L. dynatis Late Pennsylvanian; central Colorado
Family TseajaiidaeGenus Tseajaia
T. campi Early Permian, southeastern Utah; Late Pennsylvanian/Early
Permian north-central New Mexico
Family Diadectidae
DIADECTOMORPHA (continued)
Family DiadectidaeGenus Ambedus
A. pusillus Early Permian; central OhioGenus Desmatodon
D. hesperis Late Pennsylvanian; central Colorado
D. hollandi Late Pennsylvanian; PennsylvaniaGenus Diadectes
D. absitus Early Permian; central GermanyD. sanmiguelensis Early Permian; central ColoradoD. sideropelicus Early Permian; Texas, Oklahoma, Ohio(?),
southeastern Utah,Pennsylvania
D. tenuitectes Early Permian; northcentral TexasGenus Diasparactus
D. zenos Late Pennsylvanian/Early Permian; northern New Mexico
Genus OrobatesO. pabsti Early Permian; Thuringia, central
GermanyGenus Phanerosaurus
P. naumanni Early Permian; Saxony, GermanyGenus Stephanospondylus
S. pungnax Early Permian; Saxony, Germany
Of the diadectids, Ambedus is known from only a fragmentary dentary and maxilla.
Phanerosaurus and Stepahospondylus are known only from fragmentary vertebral materials from Europe. The specimens have since been lost (probably during World War II). The generic names “Oradectes” and “Silvadectes” have been proposed by one worker, but he never published his work in a refereed journal and are thus not considered valid taxonomic terms (despite his attempting to place them in Wikipedia).
Limnoscelidae: Limnoscelis
Limnoscelis is known from one complete skeleton from the Late Pennsylvanian north-central New Mexico, and a scattered bunch of elements of [probably] a single individual from the Late Pennsylvanian of central Colorado. It is known by its large caniniform teeth, and almost small alligator like size.
Tseajaiidae: Tseajaia
Tseajaia is a rare but unique diadectomorph known from the U.S. desert southwest four-corners region. It is known from one complete skeleton and another isolated skull. This has allowed reasonable reconstruction of the skull.
Diadectidae:
The diadectids are well known for being extremely robust, often very large. Highly terrestrially adapted, and amongst the earliest of high-fiber herbivores.
Diadectidae: Desmatodon: Desmatodon is known from partial material, mostly jaw material. See the isolated maxilla from the Late Pennsylvanian of Colorado below.
Diadectidae:
Diasparactus: Diasparactus is known only from one partial skeleton, but it has unique vertebral structure with very tall neural spines. The specimen shown below is mostly made of plaster, but the vertebrae and their long spines are actually real.
Diadectidae:
Diadectes: Diadectes is the best known and represented of the diadectids. It is particularly well known for very large specimens from North America, but they generally fuse the skull bones to the point that they are not useful phylogenetically. Juvenile specimens from New Mexico (not fused yet) and mature specimens from German (just plain beautifully preserved) have helped us to determine structure in the diadectids much more clearly.
Diadectidae:
Orobates: Orobates is one of the most completely preserved and best known of diadectids. It is slightly more primitive than Diadectes (also known from that locality), but still retains the herbivorous features typical of diadectids.
1 cm
Orobates pabsti, a diadectomorph–from central Germany; also possibly from North America
PALEO-BIOGEOGRAPHIC DISTRIBUTION OF
DIADECTOMORPHS
Late Pennsylvanian Limnoscelis (two species) is generally considered as the most basal of the Diadectomorpha, and they are known from Late Pennsylvanian age sediments of northcentral New Mexico, central Colorado, and southeastern Utah. See the red dots below. The earliest known diadectids are found from the Late Pennsylvanian as well, Diasparactus from north-central New Mexico, and Desmatodon from the Tri-state area of Ohio/Pennsylvania/West Virginia.
Late Pennsylvanian
Early Permian Whether the Diadectomorpha diversified in the Early Permian, or whether we have just had better luck finding them from Early Permian sediments, we do not know. However, numerous diadectids are known from the Early Permian, as well as the unique form Tseajaia known from southeastern Utah and north-central New Mexico. Diadectes is the most common of the diadectids, found in many regions of Pangea. Numerous other taxa (Ambedus, Phanerosaurus, Stephanospondylus) are known from much more fragmentary materials. Notably, Orobates is found only in central Germany, but is represented by numerous complete specimens. It is reasonable to say that diadectids have a distribution through northern Pangea.
Early Permian
